Geology of a complex kimberlite pipe (K2 pipe, Venetia Mine, South Africa): insights into conduit processes during explosive ultrabasic eruptions
Author:
Publisher
Springer Science and Business Media LLC
Subject
Geochemistry and Petrology
Link
http://link.springer.com/content/pdf/10.1007/s00445-008-0211-4.pdf
Reference55 articles.
1. Barnett WP (2004) Subsidence breccias in kimberlite pipes—an application of fractal analysis. Lithos 76:299–316
2. Barnett WP (2008) The rock mechanics of kimberlite volcanic pipe excavation. J Volcanol Geotherm Res DOI 10.1016/j.jvolgeores.2007.12.021
3. Barnett WP, Lorig L (2007) A model for stress-controlled pipe growth. J Volcanol Geotherm Res 159:108–125
4. Barton JM Jr, Barnett WP, Barton ES, Barnett M, Doorgapershad A, Twiggs A, Klemd R, Martin J, Mellonig L, Zenglein R (2003) The geology of the area surrounding the Venetia kimberlite pipes, Limpopo Belt, South Africa: a complex assembly of terranes and granitoid magmatism. South African J Geol 106:109–128
5. Brown RJ, Kavanagh J, Sparks RSJ, Tait M, Field M (2007) Mechanically disrupted and chemically weakened zones in segmented dike systems cause vent localization: evidence from kimberlite volcanic systems. Geology 35:184–188
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